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Australia has a wide variety of climates due to its large geographical size. The largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varying between grasslands and desert.
Climate classification. Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. One of the most used is the Köppen climate classification scheme first developed in 1884. [1]
Australia's annual average temperatures are projected to increase 0.4–2.0 °C above 1990 levels by the year 2030, and 1–6 °C by 2070. Average precipitation in the southwest and southeast Australia is projected to decline during this time, while regions such as the northwest may experience increases in rainfall.
Australia is located in the Southern Hemisphere. Relief map showing major rivers of Australia Climate of Australia. The Australian environment ranges from virtually pristine Antarctic territory and rainforests to degraded industrial areas of major cities. Forty distinct ecoregions have been identified across the Australian mainland and islands.
Australia's economy is strongly intertwined with the countries of East and Southeast Asia, also known as ASEAN Plus Three (APT), accounting for about 64% of exports in 2016. [46] China in particular is Australia's main export and import partner by a wide margin. [47] Australia is a member of the APEC, G20, OECD and WTO.
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, [ 1 ][ 2 ] with several later modifications by Köppen, notably in 1918 and 1936. [ 3 ][ 4 ] Later, German climatologist Rudolf Geiger (1894–1981 ...
Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Most of Australia is semi-arid or desert, making it the world's driest continent (excluding Antarctica). Australia's rainfall is mainly regulated by the movement of the alien ...
Summer rain over Melbourne, taken from Brighton Winter fog over the Melbourne city centre. Melbourne, the state capital of Victoria and the second most populous city in Australia (most populous in urban area), has a temperate oceanic climate (Köppen climate classification Cfb), [1] [2] bordering on a humid subtropical climate (Köppen climate classification Cfa), and is well known for its ...